INORGANIC NITROGEN STIMULATES METHANE OXIDATION IN COASTAL LAGOON SEDIMENTS

Q3 Environmental Science Oecologia Australis Pub Date : 2022-07-08 DOI:10.4257/oeco.2022.2602.18
A. Enrich-Prast, V. Figueiredo, F. Machado‐Silva, R. B. Peixoto, Leonardo Amora-Nogueira, Gabriela Cugler, Maria Carolina Barroso dos Santos, J. P. Felizardo, J. Valle, Davi Pedroni Barreto, Luciene Valladares, Laís Rodrigues, A. Santoro, L. Pinho, C. N. Signori, R. Pollery, E. Silva, H. Marotta
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Abstract

Methane (CH4) oxidation is a critical process to reduce CH4 emissions from aquatic environments to the atmosphere. Considering the continuous increase in nitrogen in rivers, lakes, and lagoons from human sources, we re-evaluated the still controversial potential effect of inorganic nitrogen on CH4 oxidation. Here, we approached three shallow coastal lagoons that represent great environmental heterogeneity and used slurry sediments as a model system. The addition of ammonium chloride (NH4Cl) and potassium nitrate (KNO3) significantly stimulated CH4 oxidation in the sediments of all studied lagoons, indicating the potential limitation of nitrogen for the growth of CH4 oxidizing bacteria. Our findings contrast to some previous reports, where ammonium and nitrate inhibited CH4 oxidation in sediments. Indeed, our experiment was performed in a more realistic range in relation to natural concentrations of inorganic nitrogen in aquatic systems (0.5 to 1 mM) and was opposed to extreme concentrations previously used (2 to 50 mM). Our results point to the need to further assess the connection between nitrogen inputs and CH4 budgets in aquatic sediments, considering the potential fuel for CH4 oxidation that may affect the global greenhouse gas balance
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无机氮刺激沿海泻湖沉积物中甲烷氧化
甲烷(CH4)氧化是减少水生环境向大气排放CH4的关键过程。考虑到人类来源导致河流、湖泊和泻湖中氮的持续增加,我们重新评估了无机氮对CH4氧化仍有争议的潜在影响。在这里,我们研究了三个代表着巨大环境异质性的浅海岸泻湖,并使用泥浆沉积物作为模型系统。氯化铵(NH4Cl)和硝酸钾(KNO3)的加入显著刺激了所有研究泻湖沉积物中CH4的氧化,表明氮对CH4氧化细菌生长的潜在限制。我们的发现与之前的一些报告形成了对比,在这些报告中,铵和硝酸盐抑制了沉积物中CH4的氧化。事实上,我们的实验是在与水生系统中无机氮的自然浓度(0.5至1mM)相关的更现实的范围内进行的,而不是之前使用的极端浓度(2至50mM)。我们的研究结果表明,考虑到可能影响全球温室气体平衡的CH4氧化的潜在燃料,有必要进一步评估水生沉积物中氮输入和CH4预算之间的联系
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来源期刊
Oecologia Australis
Oecologia Australis Environmental Science-Ecology
CiteScore
1.30
自引率
0.00%
发文量
49
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